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Report on Akan (Japan) — October 1995

Bulletin of the Global Volcanism Network, vol. 20, no. 10 (October 1995)
Managing Editor: Richard Wunderman.

Akan (Japan) Continued elevated seismicity

Please cite this report as:

Global Volcanism Program, 1995. Report on Akan (Japan). In: Wunderman, R. (ed.), Bulletin of the Global Volcanism Network, 20:10. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199510-285070.

Volcano Profile |  Complete Bulletin


Akan

Japan

43.384°N, 144.013°E; summit elev. 1499 m

All times are local (unless otherwise noted)


Seismicity during October, and thus far in 1995, remained slightly higher than was typical for the past several years (figure 6). The highest daily number of earthquakes during the month took place on 2 October and consisted of 33 events (recorded at Station A, 2.3 km from Ponmachineshiri Crater). The monthly total for October consisted of 395 events.

Figure (see Caption) Figure 6. The number of daily earthquakes at Akan's station A, 1 January 1987 through October 1995. Courtesy of JMA.

Geologic Background. Akan is a 13 x 24 km caldera located immediately SW of Kussharo caldera. The elongated, irregular outline of the caldera rim reflects its incremental formation during major explosive eruptions from the early to mid-Pleistocene. Growth of four post-caldera stratovolcanoes, three at the SW end of the caldera and the other at the NE side, has restricted the size of the caldera lake. Conical Oakandake was frequently active during the Holocene. The 1-km-wide Nakamachineshiri crater of Meakandake was formed during a major pumice-and-scoria eruption about 13,500 years ago. Within the Akan volcanic complex, only the Meakandake group, east of Lake Akan, has been historically active, producing mild phreatic eruptions since the beginning of the 19th century. Meakandake is composed of nine overlapping cones. The main cone of Meakandake proper has a triple crater at its summit. Historical eruptions at Meakandake have consisted of minor phreatic explosions, but four major magmatic eruptions including pyroclastic flows have occurred during the Holocene.

Information Contacts: Volcanological Division, Seismological and Volcanological Department, Japan Meteorological Agency (JMA), 1-3-4 Ote-machi, Chiyoda-ku, Tokyo 100 Japan.